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There are several speleological studies conducted on the karst topology around
Solunska Glava. It is assumed that beneath the peak there are enormous reservoirs of freshwater, which coincides with the old name for the mountain range
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The field is 1.5 km long and 500 to 1000 m wide and it is slightly sloped westwards. There is a small stream flowing through it forming a few karst lakes and then
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among the sink holes. The water that is lost on Begovo Pole appears at the springs of
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106:"Спелео нуркачи од Белгија и Македонија истражуваа кај Бабуна"
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128:"Јакупица има вода за третина Македонија"
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81:on the other side of Solunska Glava.
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89:(which translates to Wet Mountain).
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130:(in Macedonian). Archived from
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191:Geography of North Macedonia
62:, on the north side of peak
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20:View of Begovo Pole, from
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167:41.72694°N 21.41389°E
66:, located in central
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172:41.72694; 21.41389
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68:North Macedonia
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64:Solunska Glava
60:Jakupica range
22:Solunska Glava
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134:on 2011-09-28
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87:Mokra Planina
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196:Karst fields
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138:14 September
136:. Retrieved
132:the original
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112:14 September
110:. Retrieved
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79:Babuna river
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45:Fusha e Beut
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56:karst field
47:) (meaning
37:Бегово Поле
29:Begovo Pole
185:Categories
158:21°24′50″E
155:41°43′37″N
93:References
33:Macedonian
52:'s field
41:Albanian
58:on the
54:) is a
75:loses
140:2010
114:2010
24:peak
50:Bey
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31:(
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
